{"title":"针对丹纳克山地下水探索的新型凝胶胃方法","authors":"Muhammad Zuhdi, Agus Wachid","doi":"10.20414/konstan.v6i1.69","DOIUrl":null,"url":null,"abstract":"Geoelectricity is a geophysical method that conducted by injecting an electric current into the earth’s interior. This study objected to map aquifer aquifers using the geoelectric method with a Schlumberger electrode configuration consisting of 4 sounding points. The measurement results are then processed with IP2WIN software which produces a real resistivity map as a function of depth. The correlation between sounding points produces a three-dimensional real resistivity map. The results of the study located at Gunung Tunak, Lombok, West Nusa Tenggara, which consists of 4 sounding points show that the aquifer is at a depth of 66.7 meters 31, 2 meters 58, 7 meters and 34, 1 meter respectively, which are displayed comprehensively with 3 dimensional lithology map.","PeriodicalId":137476,"journal":{"name":"KONSTAN - JURNAL FISIKA DAN PENDIDIKAN FISIKA","volume":null,"pages":null},"PeriodicalIF":0.0000,"publicationDate":"2021-06-22","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"2","resultStr":"{\"title\":\"Metode Geolistrik Tahanan Jenis untuk Eksplorasi Air Tanah di Gunung Tunak\",\"authors\":\"Muhammad Zuhdi, Agus Wachid\",\"doi\":\"10.20414/konstan.v6i1.69\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Geoelectricity is a geophysical method that conducted by injecting an electric current into the earth’s interior. This study objected to map aquifer aquifers using the geoelectric method with a Schlumberger electrode configuration consisting of 4 sounding points. The measurement results are then processed with IP2WIN software which produces a real resistivity map as a function of depth. The correlation between sounding points produces a three-dimensional real resistivity map. The results of the study located at Gunung Tunak, Lombok, West Nusa Tenggara, which consists of 4 sounding points show that the aquifer is at a depth of 66.7 meters 31, 2 meters 58, 7 meters and 34, 1 meter respectively, which are displayed comprehensively with 3 dimensional lithology map.\",\"PeriodicalId\":137476,\"journal\":{\"name\":\"KONSTAN - JURNAL FISIKA DAN PENDIDIKAN FISIKA\",\"volume\":null,\"pages\":null},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2021-06-22\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"2\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"KONSTAN - JURNAL FISIKA DAN PENDIDIKAN FISIKA\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.20414/konstan.v6i1.69\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"KONSTAN - JURNAL FISIKA DAN PENDIDIKAN FISIKA","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.20414/konstan.v6i1.69","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
Metode Geolistrik Tahanan Jenis untuk Eksplorasi Air Tanah di Gunung Tunak
Geoelectricity is a geophysical method that conducted by injecting an electric current into the earth’s interior. This study objected to map aquifer aquifers using the geoelectric method with a Schlumberger electrode configuration consisting of 4 sounding points. The measurement results are then processed with IP2WIN software which produces a real resistivity map as a function of depth. The correlation between sounding points produces a three-dimensional real resistivity map. The results of the study located at Gunung Tunak, Lombok, West Nusa Tenggara, which consists of 4 sounding points show that the aquifer is at a depth of 66.7 meters 31, 2 meters 58, 7 meters and 34, 1 meter respectively, which are displayed comprehensively with 3 dimensional lithology map.
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